Page 2: Research news on seasonal ice

Seasonal ice is a transient phase of water that forms, persists, and melts on an annual or sub-annual cycle in response to periodic temperature and radiative forcing variations. As a substance, it commonly occurs as freshwater or saline ice with physical properties (crystal structure, brine volume, density, and mechanical strength) strongly modulated by temperature and impurity content. In cryospheric and planetary science, seasonal ice includes lake, river, and sea ice, as well as frost and snow that undergo regular phase transitions, influencing surface energy balance, gas exchange, and hydrological or climatic processes during their recurrent formation–melting cycles.

Antarctic sea ice hits its third-lowest winter peak on record

Antarctica's winter sea ice has hit its third-lowest peak in nearly half a century of satellite monitoring, researchers said Tuesday, highlighting the growing influence of climate change on the planet's southern pole.

When glaciers roamed Mars

The surface of Mars is known for being an extremely cold, desiccated, and irradiated place. But as its many surface features attest, the red planet was once a warmer, wetter place with flowing water and glaciers. Today, most ...

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